Rocks are all around us. You can see rocks inside your house, in your yard, on your street, on a country road, everywhere you look. Statues, chalk, marble, pencil lead, sandpaper, glass, tombstones, bricks, the walls of your room, mountains, pebbles, soil, and volcanoes are all rocks!! Rocks are used to build homes, an aluminum baseball bat, a washing machine, video games, airplanes, cars, and jewelry! Rocks aren't always solid. Sand and mud are rocks. No matter where you are, you are always close to rocks and minerals. They are fascinating and exciting, so let's begin our investigation to learn more.
Let's start at the beginning …
We'll begin with a look at the structure of the earth because that is where all rocks come from. They have been on Earth for almost 4 billion years. Geologists record time with the Geologic Time Table.
Where do rocks come from?
The Earth has 3 layers: the crust, the mantle and the core (which is subdivided into the outer and inner core.) Each layer is unique. You can find interesting details about the layers of the earth at Science Trek: The Earth.
How do we classify rocks?
There are 3 main types of rocks depending upon how they were formed in the different layers of the Earth. They are: Igneous, Sedimentary, and Metamorphic.
Sedimentary rock is weathered into many pieces of rock and soil which then settles into layers. The layers are squeezed together until they harden into rock.
Found in locations where oceans, lakes, or other bodies of water exist or once existed.
Metamorphic rock forms when igneous, sedimentary, or other metamorphic rock is changed by heat and pressure.
This type of rock is buried deep within the Earth where it is created from the heat and pressure found there.
Is hard, often contains crystals, may have bands or layers.
Examples: marble, slate, gneiss, schist
Geological Poetry
Rock On! By Cherry Carl
Rocks! Rocks! They're not the same!
Each one has its claim to fame.
Rocks are grouped in three main types:
Some have layers … some have stripes.
What makes them different, do you know?
Let's take a look at rocks on show.
This rock star is “igneous.”
It's made when earth seems furious.
Liquid rock erupts and cools,
Forming solid glasslike pools.
“Metamorphic” means some changes.
Mother Nature rearranges.
Using heat and pressure, too,
She makes old rocks appear as new.
“Sedimentary” means small pieces
That nature generally releases.
Using wind and water, too,
It makes new rocks for me and you.
Rocks! Rocks! You're not the same!
It's easy now to know your name.
This poem was written especially for Science Trek — courtesy of Cherry Carl. For additional poems on science, history, language, and holidays visit her website at: Carl's Corner
Changes
A rock can begin as one type and can change many times. In fact, rocks are always changing. However, the changes happen so slowly that they are difficult to see. We have seen above that heat and pressure can change rocks which then break down by weathering and move by erosion. It can take thousands of years for rocks to weather and erode. This process of changing is called the rock cycle.
Weathering is the process that breaks rocks down into smaller pieces. Weathering can be caused by: wind, rain, ice, running water, plant roots, chemicals, freezing and thawing.
Erosion is the movement of rock pieces from place to place. Erosion can be caused by: wind, rain, running water, waves, gravity, and moving ice.
Fascinating Facts
The heads at Mt. Rushmore are carved out of an igneous rock called granite.
The heat of lightning striking the beach sand can melt the sand to form a glassy rock called “fulgurite.”
Melted rock is called magma when it is inside the earth, but called lava when it runs out onto the surface of the earth.
The mineral, salt, was so valuable in ancient times that it was traded ounce for ounce for gold.
A diamond is the hardest mineral.
Meteorites are rocks from space, and they can help scientists learn about the solar system.
What else do we know about rocks?
A rock is a material made of one or more minerals. Minerals are made from 92 elements that join together in many different ways. Some minerals are made of only one element, such as silver. Most are a combination of two or more elements, such as granite which is made of quartz, feldspar, and mica.
Scientists have identified over 3,000 minerals. The particles of minerals are arranged in a repeating pattern called a crystal.
Recognizing a mineral is not an easy job. There are several different properties of minerals and tests that are used to identify them. The properties are: luster, hardness, color, streak, cleavage, crystal shape, and magnetism.
Stalactites and Stalagmites
Stalactites form when mineral deposits and water seep from the walls, ceilings, or rocks inside caves. These deposits drip slowly and create an icicle-type formation. To remember the difference between these two formations, think: stalactites "stick tight."
Stalagmites are the collection of mineral deposits that build up on the floor of a cave. The dripping minerals stack on top of previous deposits to form a type of tower. Sometimes they connect with stalactites to form a column.
Spelunking
People who visit caves for the sport of enjoying the stalactites, stalagmites and other rock and mineral formations that can be found there are known as spelunkers. Visit this Spelunking Basics site to learn more about spelunking.
Volcanoes
The crust of the earth is solid and is broken into giant chunks that float on the hot, liquid mantle. These chunks are called tectonic plates. Our continents rest on them. At times the mantle can actually find a crack or weak spot in the earth's crust and break out to the surface of the earth. It is here that the melted rocks, or magma, can erupt through the crust. When the magma escapes the heat and pressure that has built up under the earth's surface through a vent in the crust, it is called a volcano. When cooled, the lava forms igneous rocks. Learn more about volcanoes at Science Trek's Volcanoes site.
Earthquakes
The earth's tectonic plates, floating on the mantle layer, often slide or bump against each other. When that happens, the earth beneath us shakes. A fault or crack in the earth's surface is often the primary location of many earthquakes. The point where that shaking happens takes place below the surface. This strong collision happens at a location known as the focus. Just above the focus, on the earth's surface, is the epicenter of an earthquake. The earthquake shakes the ground in waves that can be measured by scientists known as seismologists. The Richter Scale, an instrument for identifying the strength of an earthquake, works by measuring the seismic waves. Learn more about earthquakes at Science Trek's Earthquakes site.
Want to learn more about the rock cycle?
The rock cycle is complex, but you can learn a lot by revisiting the idea of it over and over. Check out these sites for more information:
The Mineralogical Society of America has a rockin' Mineralogy4Kids site
Learner.org has a great interactive page to study the rock cycle
